2008
DOI: 10.2495/friar080121
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History of flood fighting in the Kisosansen River Basin

Abstract: The Isewan Typhoon caused considerable damage to the downstream regions of the Kisosansen River Basin on 26 th September 1959. It caused approximately 4,500 deaths in and around Nagoya City, the most industrial city in Japan. This study describes the history surrounding the major flood mitigation projects related to land use in the Kisosansen River Basin since 100 A.D. when paddy fields were first established on the alluvial plain. Land use of the area gradually evolved to cover the entire alluvial plain, deve… Show more

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“…Spur dikes are structures that are built perpendicular or diagonally to the river channel, mainly in the middle and lower reaches of rivers, to prevent riverbank erosion [34]. They were first introduced in Japan by Dutch engineers in the 1800s (Meiji era) and were used for the channelization of large rivers in low-lying areas, like the Kiso River [5,35]. They were later introduced to steep rivers on alluvial fans, like the Kurobe River [36].…”
Section: Spur Dike Applicationsmentioning
confidence: 99%
“…Spur dikes are structures that are built perpendicular or diagonally to the river channel, mainly in the middle and lower reaches of rivers, to prevent riverbank erosion [34]. They were first introduced in Japan by Dutch engineers in the 1800s (Meiji era) and were used for the channelization of large rivers in low-lying areas, like the Kiso River [5,35]. They were later introduced to steep rivers on alluvial fans, like the Kurobe River [36].…”
Section: Spur Dike Applicationsmentioning
confidence: 99%
“…The channel gradient was 0.15% with an average wetted main-channel width of c. 400 m during the base-flow period. The natural functional floodplain of Kiso River has been reduced substantially over the past few hundred years, with constructions of flood dykes that run along both sides of the segment (Takeuchi, Takezawa & Gotoh, 2008). Relatively extensive areas of gravel and sand bars without or with sparse vegetation cover remained within dykes in the 1930s, within which large numbers of floodplain backwaters (i.e.…”
Section: Study Sitementioning
confidence: 99%